TY - JOUR
T1 - Characterization of water-soluble brown carbon chromophores from wildfire plumes in the western USA using size-exclusion chromatography
AU - Azzarello, Lisa
AU - Washenfelder, Rebecca A.
AU - Robinson, Michael A.
AU - Franchin, Alessandro
AU - Womack, Caroline C.
AU - Holmes, Christopher D.
AU - Brown, Steven S.
AU - Middlebrook, Ann
AU - Newberger, Tim
AU - Sweeney, Colm
AU - Young, Cora J.
N1 - Publisher Copyright:
© 2023 Lisa Azzarello et al.
PY - 2023/12/20
Y1 - 2023/12/20
N2 - Wildfires are an important source of carbonaceous aerosol in the atmosphere. Organic aerosol that absorbs light in the ultraviolet to visible spectral range is referred to as brown carbon (BrC), and its impact on Earth's radiative budget has not been well characterized. We collected water-soluble brown carbon using a particle-into-liquid sampler (PILS) on board a Twin Otter aircraft during the Fire Influence on Regional to Global Environments and Air Quality (FIREX-AQ) campaign. Samples were collected downwind of wildfires in the western United States from August to September 2019. We applied size-exclusion chromatography (SEC) with ultraviolet-visible spectroscopy to characterize the molecular size distribution of BrC chromophores. The wildfire plumes had transport ages of 0 to 5h, and the absorption was dominated by chromophores with molecular weights <500Da. With BrC normalized to a conserved biomass burning tracer, carbon monoxide, a consistent decrease in BrC absorption with plume age was not observed during FIREX-AQ. These findings are consistent with the variable trends in BrC absorption with plume age reported in recent studies. While BrC absorption trends were broadly consistent between the offline SEC analysis and the online PILS measurements, the absolute values of absorption and their spectral dependence differed. We investigate plausible explanations for the discrepancies observed between the online and offline analyses. This included solvent effects, pH, and sample storage. We suspect that sample storage impacted the absorption intensity of the offline measurements without impacting the molecular weight distribution of BrC chromophores.
AB - Wildfires are an important source of carbonaceous aerosol in the atmosphere. Organic aerosol that absorbs light in the ultraviolet to visible spectral range is referred to as brown carbon (BrC), and its impact on Earth's radiative budget has not been well characterized. We collected water-soluble brown carbon using a particle-into-liquid sampler (PILS) on board a Twin Otter aircraft during the Fire Influence on Regional to Global Environments and Air Quality (FIREX-AQ) campaign. Samples were collected downwind of wildfires in the western United States from August to September 2019. We applied size-exclusion chromatography (SEC) with ultraviolet-visible spectroscopy to characterize the molecular size distribution of BrC chromophores. The wildfire plumes had transport ages of 0 to 5h, and the absorption was dominated by chromophores with molecular weights <500Da. With BrC normalized to a conserved biomass burning tracer, carbon monoxide, a consistent decrease in BrC absorption with plume age was not observed during FIREX-AQ. These findings are consistent with the variable trends in BrC absorption with plume age reported in recent studies. While BrC absorption trends were broadly consistent between the offline SEC analysis and the online PILS measurements, the absolute values of absorption and their spectral dependence differed. We investigate plausible explanations for the discrepancies observed between the online and offline analyses. This included solvent effects, pH, and sample storage. We suspect that sample storage impacted the absorption intensity of the offline measurements without impacting the molecular weight distribution of BrC chromophores.
UR - https://www.scopus.com/pages/publications/85182996459
U2 - 10.5194/acp-23-15643-2023
DO - 10.5194/acp-23-15643-2023
M3 - Article
AN - SCOPUS:85182996459
SN - 1680-7316
VL - 23
SP - 15643
EP - 15654
JO - Atmospheric Chemistry and Physics
JF - Atmospheric Chemistry and Physics
IS - 24
ER -